Submarine carbonate breccia beds—a oppositional model for two-layer, sediment gravity flows from the Sekwi Formation (Lower Cambrian), Mackenzie Mountains, Northwest Territories, Canada
- 1 January 1979
- journal article
- Published by Canadian Science Publishing in Canadian Journal of Earth Sciences
- Vol. 16 (1), 189-199
- https://doi.org/10.1139/e79-017